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Erosion Rates on Mars and Implications for Climate Change: Constraints From the Pathfinder Landing Site

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dc.contributor.author Golombek, M. en_US
dc.contributor.author Bridges, N. en_US
dc.date.accessioned 2004-09-24T16:33:35Z
dc.date.available 2004-09-24T16:33:35Z
dc.date.issued 1999 en_US
dc.identifier.citation Journal of Geophysical Research, Planets en_US
dc.identifier.citation USA en_US
dc.identifier.clearanceno 99-1338 en_US
dc.identifier.uri http://hdl.handle.net/2014/17888
dc.description.abstract The observation that the Mars Pathfinder landing site looks very similar to its apperance after it was deposited by catastrophic floods some 1.8-3.5 Ga allows quantitative constraints to be placed on the rate of change of the site since that time. en_US
dc.format.extent 3013575 bytes
dc.format.mimetype application/pdf
dc.language.iso en_US
dc.subject.other Erosion Mars Climate change en_US
dc.title Erosion Rates on Mars and Implications for Climate Change: Constraints From the Pathfinder Landing Site en_US


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